2008 Vol.57 No.9 総説 佐野有司
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1 Reprinted from RADIOISOTOPES, Vol.57,.9 September 2008 Japan Radioisotope Association http : //
2 µ µ µ µ µ
3 µ µ µ µ µ t λ t λ t λ λ
4 λ t λ t t
5 µ µ µ µ
6 µ
7
8 µ µ
9 M M M M M M M M
10 σ µ σ µ µ µ
11 588 RADIOISOTOPES Vol 5 7 No 9 囲で一致するので 海水中で成長したことを示 す そして 最外苑部で再び海水より高い値を 示す この結果は アユ個体が淀川で捕獲され た事実と一致する このように 概ねアユの生 態に沿ったストロンチウム同位体比の変動が得 られた この分析法は海と河川を回遊する他の 魚類 サケやウナギに応用可能であり 将来は 水産学に貢献するものであろう 4 お わ り に 本総説では 近年 東京大学海洋研究所に設 置された二次元高分解能二次イオン質量分析計 NanoSIMS を用いた直径約5 µ m の ス ポ ッ トでの鉛とストロンチウムの同位体測定法とそ の応用について概説した これらの元素は共に 放 射 性 起 源 の 安 定 同 位 体 206Pb 207Pb 87Sr 等 を含むために 天然における同位体比の変 動が大きく プローブ径を5 µ m まで絞っても 誤差の範囲を超えた有意な変動が得られた そ して モナザイト中の鉛同位体分析では 鉱物 の形成年代という地質学における重要な情報が 求められた 一方 耳石 アラゴナイト 中の ストロンチウム同位体分析では アユの回遊に 図7 a アユ耳石の中心から分析スポットまでの距 離とストロンチウム/カルシウム比の関係を示 した図と b 距離とストロンチウム同位体比の 図 網掛けの部分は琵琶湖 大阪湾 淀川の 文献値を示す ついての生態情報を引き出すことが可能となっ た このように 微小領域の安定同位体分析法 は 今後地質学 水産学に加えてさまざまな分 野に応用できる可能性を秘めている 文 同位体比 図7b を見ると ストロンチウム 献 濃度が低いために測定誤差が大きくなっている 1 Suzuki, K. and Adachi, M., Precambrian prove- 7125 が 中 心 か ら1 00 µ m ま で の 平 均 値 は0 nance and Silurian metamorphism of the Tsubo- ±0 0009と海水の値 0 709 2 以下の括弧 内 nosawa paragneiss in the South Kitakami terrane, Northeast Japan, revealed by Th-U-total 0001より小さい より の値の誤差は2 σ で0 Pb chemical isochron ages of monazite, zircon 明らかに高く 琵琶湖 0 7119 や淀川 0 7115 and xenotime, Geochem. J., 25, と一致する したがって このアユは耳石が 2 Montel, J. M., Foret, S., Veschambre, M., Nicollet, 100 µ m まで成長する間は 琵琶湖あるいは淀 N. and Provost, A., Electron microprobe dating of monazite, Chem. Geol., 131, 川に生息していたのであろう Sr/Ca 比とは逆 50 µ m に 100 µ m を過ぎると急激に低下し 1 3 Hirata, T. and Nesbitt, R. W., U Pb isotope geo- で最低値に達した後で徐々に上昇する傾向にあ る これらの87Sr/86Sr 比は海水の値と誤差の範 32 chronology of zircon Evaluation of the laser probe-inductively coupled plasma-mass spec-
12 Geochim. Cosmochim. Acta Chem. Geol Geology J. Anal. At. Spectrom Int. J. Mass Spectr J. Geophys. Res. B89 Suppl Geochim. Cosmochim. Acta, J. Analytical Atomic Spectrometry Geochim. Cosmochim. Acta Science, Geochim. Cosmochim Acta Geophys. Res. Lett Analy. Sci Geochem. J App. Geochem
13 Earth Planet. Sci. Lett Earth Planet. Sci. Lett Trans. Amer. Geophys. Union Science Geochim. Cosmochim. Acta Chem. Geol Hydrol. Process Appl. Geochem Sci. Total Environ Geostandards Newsletter, Geochim. Cosmochim. Acta Chem. Geol Terra Nova Bull. Fish. Res. Agency Suppl Mar. Ecol. Prog. Ser The method of and isotope measurements at about 5 µmresolution was developed by using a high lateral resolution secondary ion mass spectrometer. Sincethe both elements have radiogenic nuclides such as,, and, natural variations of isotopic ratios are large. It is possible to detect a meaningful variation in a terrestrial sample, even though the experimental error is relatively large. In the case of monazite dating, a 4 primary beam
14 was used to sputter the sample and secondary positive ions were extracted for mass analysis using a Mattauch Herzog geometry. The multi collector system was modified to detect,,,, and ions simultaneously. Based on the monazite standard from North Central Madagascar, we have determined the ratios of samples. ratios were measured by a magnet scanning with a single collector mode. 44 monazite grains extracted from a sedimentary rock in Taiwan were analyzed. Observed ages were consistent with the chemical ages by EPMA. Then NanoSIMS has been used to measure ratios in natural calcium carbonate samples. Multi collector system at the same time. Magnetic field was scanning for the counter to detect, and,while the can measure,, and, respectively. Repeated analyses of a coral skeleton standard show that / ratio agrees well with the seawater signature, after the series of corrections such as dimer,, andamass bias estimated by / ratio. The method is applied to an otolith from ayu (Plecoglossus altivelis altivelis) collected from the Yodo river, Japan. The spatial variation of / ratios was consistent with amphidromous migration of the fish, namely, born in the lake and grown in the coastal sea and finally collected in a river. was adjusted to detect,,,
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